LECTURE 4
The state of the system is described by its
properties.
Once a sufficient number of properties are
specified, the rest of the properties assume some values automatically.
The number of properties required to fix a
state of a system is given by the state postulate:
The
state of a simple compressible system is completely specified by two
independent, intensive properties.
The system is called a simple compressible system in the absence of electrical, magnetic, gravitational, motion, and
surface tension effects.
The state
postulate requires that the two
properties specified be independent to fix the state.
Two properties are independent if one property
can be varied while the other one is held constant.
Temperature and specific volume, for example,
are always independent properties, and together they can fix the state of a
simple compressible system.
Thus, temperature and pressure are not
sufficient to fix the state of a two-phase system.
Otherwise an additional property needs to be
specified for each effect that is significant.
An additional property needs to be specified
for each other effect that is significant.
We cannot assign numerical values to
temperatures based on our sensations alone. Furthermore, our senses may be
misleading.
Several
properties of material changes with temperature in a repeatable and predictable
way, and this forms the basis of accurate temperature measurement.
The commonly
used mercury-in-glass thermometer for example, is based on the expansion of
mercury with temperature.
Temperature is also measured by using several other temperature
dependant properties.
Two
bodies (eg. Two copper blocks) in contact attain thermal equilibrium when the
heat transfer between them stops.
The equality of temperature is the only
requirement for thermal equilibrium.
In thermodynamics,
it is very desirable to have a temperature scale that is independent of the
properties of the substance or substances.
Such a temperature scale is called a thermodynamic
temperature scale.(Kelvin in SI)
The temperatures on
this scale are measured using a constant volume thermometer.
Based
on the principle that at low pressure, the temperature of the gas is
proportional to its pressure at constant volume.
The relationship
between the temperature and pressure of the gas in the vessel can be expressed
as
Where the values of the constants a and b
for a gas thermometer are determined experimentally.
Once a
and b are known, the temperature of a medium can be calculated from the
relation above by immersing the rigid vessel of the gas thermometer into the
medium and measuring the gas pressure.
Ideal gas temperature scale can be developed by
measuring the pressures of the gas in the vessel at two reproducible points
(such as the ice and steam points) and assigning suitable values to
temperatures those two points.
Considering
that only one straight line passes through two fixed points on a plane, these
two measurements are sufficient to determine the constants a and b
in the above equation.
If the ice and the steam points are assigned
the values 0 and 100 respectively, then the gas temperature scale will be
identical to the Celsius scale.
In this
case, the value of the constant a (that corresponds to an absolute
pressure of zero) is determined to be –273.150C when extrapolated.
The equation reduces to T = bP, and thus we need to
specify the temperature at only one point to define an absolute gas temperature
scale.
Absolute gas temperature is identical to thermodynamic temperature
in the temperature range in which the gas thermometer can be used.
We can view that thermodynamic temperature scale at
this point as an absolute gas temperature scale that utilizes an ideal gas that
always acts as a low-pressure gas regardless of the temperature.
At the Tenth international conference on weights and
measures in 1954, the Celsius scale has been redefined in terms of a single
fixed point and the absolute temperature scale.
The
triple point occurs at a fixed temperature and pressure for a specified
substance.
The selected
single point is the triple point
of water (the state in which all three phases of water coexist in equilibrium),
which is assigned the value 0.01 C. As before the boiling point of water
at 1 atm. Pressure is 100.0 C. Thus the
new Celsius scale is essentially the same as the old one.
On the
Kelvin scale, the size of Kelvin unit is defined as “ the fraction of 1/273.16
of the thermodynamic temperature of the triple point of water, which is
assigned a value of 273.16K”. The ice point on Celsius and Kelvin are
respectively 0 and 273.15 K.